This page is the "no surprises" drill for the speed-of-sound formula . We take
a = γ R T
and push it through every kind of case an exam or a real wing can throw at you: normal air, cold air, other gases, degenerate inputs (what happens as T → 0 ?), the classic Newton mistake, ratios, and a word problem. Before each example you make a Forecast — guess the answer's ballpark first, then check yourself.
Every problem about a = γ R T falls into one of these cells. The worked examples below each carry a tag telling you which cell they nail.
#
Case class
What changes
Example
A
Baseline — standard sea-level air
nothing (reference case)
Ex 1
B
Cold input — lower T
T ↓⇒ a ↓
Ex 2
C
Different gas — new γ , R , M
swap all three constants
Ex 3
D
Ratio / relative — compare two states
constants cancel, only T ratio survives
Ex 4
E
Degenerate / limiting — T → 0 , T → ∞
boundary behaviour
Ex 5
F
Wrong process trap — isothermal vs adiabatic
the γ / Newton error
Ex 6
G
Unit trap — Celsius, or universal R
catch the classic slip
Ex 7
H
Real-world word problem — Mach + altitude
chain a into M
Ex 8
I
Exam twist — solve backwards for T
invert the formula
Ex 9
Worked example Example 1 — Baseline: sea-level air
(cell A)
Find a in dry air at T = 288 K , with γ = 1.4 , R = 287 J k g − 1 K − 1 .
Forecast: you've probably heard "about 340 m/s" — guess that.
Multiply the three numbers under the root: 1.4 × 287 × 288 = 115 , 718 .
Why this step? The formula a 2 = γ R T says the square of the answer is this product; we build a 2 first.
Take the square root: a = 115 , 718 ≈ 340 m/s .
Why this step? a , not a 2 , is what we want; the root undoes the square.
Verify: units are 1 ⋅ kg K J ⋅ K = kg J = kg kg m 2 / s 2 = m 2 / s 2 = m/s . ✓ It's a speed, and ≈ 340 matches everyday experience.
Worked example Example 2 — Cold input at cruise altitude
(cell B)
At 11 km the air is T = 217 K . Same air constants. Find a .
Forecast: colder gas → slower sound. So less than 340. Guess ~290–300.
Product: 1.4 × 287 × 217 = 87 , 176 .
Why this step? Only T changed; the constants stay, so we just rebuild a 2 with the new T .
Root: a = 87 , 176 ≈ 295 m/s .
Why this step? Same reason as before — undo the square.
Verify: 295 < 340 ✓ (colder → slower, as forecast). Also 340 295 = 217/288 = 0.753 = 0.868 ✓ — consistent with cell D's ratio rule below.
Worked example Example 3 — Different gas: helium
(cell C)
Helium at T = 288 K : γ ≈ 1.667 , molar mass M = 4 g/mol so R = R u / M = 8314/4 = 2078 J k g − 1 K − 1 .
Forecast: helium is much lighter than air (M = 4 vs 29), so R is huge — sound should be way faster than 340. Guess ~1000.
Compute the specific R : 8314/4 = 2078 .
Why this step? a uses the specific constant (per kg), and lighter molecules make it larger — this is the whole reason helium is fast.
Product: 1.667 × 2078 × 288 = 997 , 700 (approx).
Why this step? Rebuild a 2 with helium's own three constants.
Root: a = 997 , 700 ≈ 999 m/s .
Verify: 999 ≫ 340 ✓. This is why your voice squeaks on helium — the medium carries pressure pulses ~3× faster. See Ideal gas law and specific gas constant .
Worked example Example 4 — Ratio of two states (constants cancel)
(cell D)
Same gas, two temperatures T 1 = 288 K and T 2 = 320 K . Find a 2 / a 1 without computing either speed.
Forecast: warmer → faster, so ratio > 1 , and only slightly (since it's a square root of the T-ratio, changes are gentle).
Write a 1 a 2 = γ R T 1 γ R T 2 = T 1 T 2 .
Why this step? γ and R are identical in both, so they cancel — a ratio problem only ever cares about T .
Plug in: 320/288 = 1.111 = 1.054 .
Why this step? Now it's one square root, no gas constants needed.
Verify: a ∝ T , so a + 11% temperature rise gives only a + 5.4% speed rise — square roots soften changes, matching the "gentle" forecast. ✓
Worked example Example 5 — Degenerate & limiting inputs
(cell E)
What is a as T → 0 K ? And what does T → ∞ imply? Use air constants where numbers help.
Forecast: at absolute zero molecules stop moving, so nothing carries a push — guess a → 0 . At huge T , a grows without bound (but slowly, like T ).
Limit T → 0 : a = γ R ⋅ 0 = 0 .
Why this step? The product under the root vanishes; a zero factor kills it. Physically: no thermal molecular motion → no carrier for the wave.
Limit T → ∞ : a = γ R T → ∞ , but it rises like T , so slowly — doubling T multiplies a by only 2 ≈ 1.41 .
Why this step? The exponent 2 1 controls how fast a limit blows up; it's sub-linear, so no runaway.
Sanity numbers: at T = 1152 K (=4 × 288 ), a = 1.4 ⋅ 287 ⋅ 1152 = 462 , 872 ≈ 680 m/s — exactly 2 × 340 , since 4 = 2 .
Verify: the T = 0 answer is 0 ✓ (no negative or complex speed — always physical because T ≥ 0 in kelvin). The 4 × T giving 2 × a confirms the T scaling. ✓
Worked example Example 6 — The wrong-process trap: Newton vs Laplace
(cell F)
Compute the isothermal (Newton) speed a iso = R T and the correct adiabatic (Laplace) speed a = γ R T at T = 288 K . By what percent is Newton wrong?
Forecast: Newton dropped the γ , so his number is smaller by a factor γ = 1.4 ≈ 1.18 . Expect ~15% too low.
Newton: a iso = 287 × 288 = 82 , 656 ≈ 287.5 m/s .
Why this step? Isothermal p = ρR T gives d p / d ρ = R T , no γ — this is exactly the tempting error from the parent note.
Laplace (correct): a = 1.4 × a iso = 1.183 × 287.5 ≈ 340 m/s .
Why this step? The real wave is adiabatic , multiplying a 2 by γ , i.e. a by γ .
Error: 340 340 − 287.5 = 0.154 = 15.4% too low.
Verify: the two speeds differ by exactly 1.4 = 1.183 ✓, and 287.5 m/s is Newton's famous ~15% miss. ✓
Worked example Example 7 — Unit traps: Celsius & universal
R (cell G)
A student writes a = 1.4 × 8.314 × 15 for "air at 1 5 ∘ C". What two mistakes are there, and what is the correct value?
Forecast: using R u = 8.314 instead of 287 makes the number ~287/8.314 ≈ 5.9 × too small, and 15 K instead of 288 K makes it wildly wrong too. Their answer will be nonsense (tens of m/s).
Their (wrong) value: 1.4 × 8.314 × 15 = 174.6 ≈ 13.2 m/s .
Why this step? Show how far off the double error lands — nowhere near a real sound speed.
Fix the temperature: 1 5 ∘ C = 15 + 273 = 288 K .
Why this step? The formula needs absolute temperature; Celsius has a false zero.
Fix the constant: use R = 287 (specific), not R u = 8.314 (universal).
Why this step? a is per-kilogram physics; R u is per-mole. Divide by molar mass first: 8314/29 ≈ 287 .
Correct value: 1.4 × 287 × 288 ≈ 340 m/s .
Verify: the wrong answer (13.2 ) is absurd (a bicycle is faster) ✓; the corrected one is 340 ✓.
Worked example Example 8 — Real-world word problem: Mach at altitude
(cell H)
A jet cruises at a true airspeed V = 250 m/s at 11 km where T = 217 K . Is it in the compressible regime? See Compressibility and why M > 0.3 matters .
Forecast: sound at altitude is slow (~295 from Ex 2), so M = 250/295 is comfortably above 0.3 — yes, compressible; probably high-subsonic ~0.85.
Local sound speed: a = 1.4 × 287 × 217 ≈ 295 m/s (from Ex 2).
Why this step? Mach uses the local a , set by the local temperature — not the sea-level value.
Mach number: M = a V = 295 250 ≈ 0.847 .
Why this step? M = V / a compares the plane's speed to how fast pressure signals travel; it decides whether density changes matter.
Compare to thresholds: 0.847 > 0.3 → compressible, and < 1 → still subsonic .
Verify: M ≈ 0.85 ✓ — a realistic airliner cruise Mach. Note the same 250 m/s at sea level (a = 340 ) gives M = 0.74 : at altitude the same speed is "more transonic" because a dropped. ✓
Worked example Example 9 — Exam twist: solve backwards for
T (cell I)
A microphone measures a = 350 m/s in air. What was the air temperature?
Forecast: 350 is a touch above the 340 -at-288 -K baseline, so T should be a little above 288 K, maybe ~305 K.
Start from a 2 = γ R T and isolate T : T = γ R a 2 .
Why this step? We're given the output ; algebra inverts the formula to recover the input .
Plug in: T = 1.4 × 287 35 0 2 = 401.8 122 , 500 ≈ 305 K .
Why this step? Divide the measured a 2 by the fixed constants to peel back to temperature.
Verify: 305 K = 3 2 ∘ C , a warm day — reasonable ✓. Re-forward-check: 1.4 × 287 × 305 = 122 , 549 ≈ 350 ✓, closing the loop.
Recall Cover the answers — did you hit every cell?
How does a change if only T falls? ::: It drops, as a ∝ T (cell B/D).
Ratio of sound speeds at T 2 and T 1 ? ::: T 2 / T 1 — constants cancel (cell D).
What is a as T → 0 K ? ::: 0 — no thermal motion to carry the wave (cell E).
Newton's isothermal error is how large? ::: ~15% too low; he dropped the γ factor (cell F).
Two classic unit slips? ::: Celsius instead of kelvin; universal R u instead of specific R (cell G).
To get T from a measured a ? ::: T = a 2 / ( γ R ) (cell I).
"Root the T, halve the wobble" — since a ∝ T , temperature changes shrink to half their percentage in a .